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SO2 oxidation products other than H2SO4 as a trigger of new particle formation ? Part 2: Comparison of ambient and laboratory measurements, and atmospheric implications

Publikováno v: Atmospheric Chemistry and Physics Discussions
Atmospheric Chemistry and Physics Discussions, 2008, 8 (3), pp.9673-9695
Atmospheric Chemistry and Physics, Vol 8, Iss 23, Pp 7255-7264 (2008)
Atmospheric Chemistry and Physics Discussions, European Geosciences Union, 2008, 8 (3), pp.9673-9695

International audience; Atmospheric new particle formation is generally thought to occur due to homogeneous or ion-induced nucleation of sulphuric acid. We compare ambient nucleation rates with laboratory data from nucleation experiments involving ei

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::ee86deaa93b9622363f6ca896b1d01d6
https://hal.science/hal-00304191/document

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The role of VOC oxidation products in continental new particle formation

Autor: Laaksonen, A., M. Kulmala, C. D. O'Dowd, J. Joutsensaari, P. Vaattovaara, S. Mikkonen, K.E.J. Lehtinen, L. Sogacheva, M. Dal Maso, P. Aalto, T. Petäjä, A. Sogachev, Y. J. Yoon, H. Lihavainen, D. Nilsson, M. C. Facchini, F. Cavalli, S. Fuzzi, T. Hoffmann, Arnold, F, Hanke, M, Sellegri, K, Umann, B, Junkermann, W, Coe, H, Allan, JD, Alfarra, MR, Worsnop, DR, Riekkola, ML, Hyotylainen, T, Viisanen, Y

Publikováno v: Atmospheric chemistry and physics
8 (2008): 2657–2665.
info:cnr-pdr/source/autori:Laaksonen, A., M. Kulmala, C. D. O'Dowd, J. Joutsensaari, P. Vaattovaara, S. Mikkonen, K.E.J. Lehtinen, L. Sogacheva, M. Dal Maso, P. Aalto, T. Petäjä, A. Sogachev, Y. J. Yoon, H. Lihavainen, D. Nilsson, M. C. Facchini, F. Cavalli, S. Fuzzi, T. Hoffmann, Arnold, F; Hanke, M; Sellegri, K; Umann, B; Junkermann, W; Coe, H; Allan, JD; Alfarra, MR; Worsnop, DR; Riekkola, ML; Hyotylainen, T; Viisanen, Y/titolo:The role of VOC oxidation products in continental new particle formation/doi:/rivista:Atmospheric chemistry and physics (Print)/anno:2008/pagina_da:2657/pagina_a:2665/intervallo_pagine:2657–2665/volume:8

Aerosol physical and chemical properties and trace gas concentrations were measured during the QUEST field campaign in March-April 2003, in Hyytiala, Finland. Our aim was to understand the role of oxidation products of VOC's such as mono- and sesquit

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::2cd70f01e0e265f011d1bc711f2a0335
https://publications.cnr.it/doc/45108

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Atmosphärische Untersuchungen der Wechselwirkung von Mineralstaub mit den Spurengasen HNO 3 und SO 2

Autor: Umann, B.

The trace gases HNO3 and SO2 have an influence on various atmospheric processes concerning the earths climate. Mineral dust, one of the most abundant aerosols in the atmosphere, may have a lasting but almost unexplored effect on their concentrations.

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od______1874::6a0c38518560f4016fbc858cede55d7e
https://hdl.handle.net/11858/00-001M-0000-0011-8BD7-F11858/00-001M-0000-0011-8BD6-2

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Atmospheric measurements of gas-phase HNO3 and SO2 using chemical ionization mass spectrometry during the MINATROC field campaign 2000 on Monte Cimone

Autor: Hanke, M., Umann, B., Uecker, J., Arnold, F., Bunz, B.

Publikováno v: Atmospheric Chemistry and Physics
Atmospheric Chemistry and Physics, European Geosciences Union, 2003, 3 (2), pp.417-436
Atmospheric Chemistry and Physics, Vol 3, Iss 2, Pp 417-436 (2003)

International audience; The EU-project MINATROC (MINeral dust And TROpospheric Chemistry) aims at enabling an estimation of the influence of mineral dust, a major, but to date largely ignored component of tropospheric aerosol, on tropospheric oxidant

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::a7cfda96c0d0784c7fa4535a5db260a2
https://hal.science/hal-00295250

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